intermediate water

简明释义

中层水 (在上层与深层水之间约一百米深

英英释义

例句

1.The intermediate water 中层水 layer can affect nutrient distribution in the ocean.

中层水 intermediate water 层可以影响海洋中的营养分布。

2.The intermediate water 中层水 is often affected by both surface and deep water currents.

中层水 intermediate water 通常受到表层和深层水流的影响。

3.Scientists are studying the properties of intermediate water 中层水 to predict climate change effects.

科学家们正在研究中层水 intermediate water 的特性，以预测气候变化的影响。

4.The research team found that the intermediate water 中层水 layer plays a crucial role in ocean circulation.

研究小组发现，中层水 intermediate water 层在海洋循环中起着至关重要的作用。

5.During the experiment, we measured the temperature of the intermediate water 中层水 to understand its impact on marine life.

在实验过程中，我们测量了中层水 intermediate water 的温度，以了解其对海洋生物的影响。

作文

The concept of intermediate water refers to a specific layer of water in the ocean that exists between the surface and deep water layers. This layer is characterized by its unique physical and chemical properties, which distinguish it from both the upper and lower layers of the ocean. Understanding intermediate water is crucial for marine scientists as it plays a significant role in ocean circulation, climate regulation, and marine ecosystems.In the context of oceanography, intermediate water typically forms at certain latitudes where temperature and salinity conditions create a stable layer. For instance, the North Atlantic Intermediate Water is formed when cold, dense water sinks and spreads out at depths ranging from approximately 200 to 1,500 meters. This process is essential for the global conveyor belt of ocean currents, which helps regulate the Earth's climate by distributing heat around the planet.Moreover, intermediate water serves as a habitat for various marine species. Many fish and other organisms thrive in this layer due to the availability of nutrients and the relatively stable environment. The presence of intermediate water is also indicative of the health of marine ecosystems. Changes in its temperature or salinity can have significant impacts on marine life, leading to shifts in species distributions and abundances.Research on intermediate water has gained increasing importance in recent years, particularly in light of climate change. As global temperatures rise, the characteristics of ocean waters are changing, affecting the formation and stability of intermediate water. This can lead to alterations in ocean circulation patterns, which may have far-reaching consequences for weather systems and marine biodiversity.In conclusion, the study of intermediate water is vital for understanding the complexities of our oceans and their interactions with the atmosphere. By examining this intermediate layer, scientists can gain insights into broader environmental changes and their implications for both marine life and human societies. Therefore, further research and monitoring of intermediate water are essential in addressing the challenges posed by climate change and ensuring the sustainability of our oceans for future generations.

“中层水”这一概念指的是海洋中位于表层水和深层水之间的特定水层。该水层具有独特的物理和化学性质，这使其与海洋的上下层水相区别。理解中层水对海洋科学家至关重要，因为它在海洋循环、气候调节和海洋生态系统中扮演着重要角色。在海洋学的背景下，中层水通常在某些纬度形成，其温度和盐度条件创造了一个稳定的水层。例如，北大西洋中层水是在大约200到1500米深度处，寒冷、密度大的水下沉并扩散时形成的。这个过程对于全球海洋洋流的输送带至关重要，帮助调节地球的气候，通过在地球上分配热量。此外，中层水为各种海洋物种提供栖息地。许多鱼类和其他生物在这一水层中繁衍生息，因为这里营养丰富且环境相对稳定。中层水的存在也表明海洋生态系统的健康状况。其温度或盐度的变化可能对海洋生物产生显著影响，导致物种分布和丰度的变化。近年来，关于中层水的研究变得越来越重要，特别是在气候变化的背景下。随着全球气温的上升，海洋水体的特性正在发生变化，影响着中层水的形成和稳定性。这可能导致海洋循环模式的改变，从而对天气系统和海洋生物多样性产生深远的影响。总之，研究中层水对于理解我们海洋的复杂性及其与大气的相互作用至关重要。通过研究这一中间层，科学家可以深入了解更广泛的环境变化及其对海洋生物和人类社会的影响。因此，进一步研究和监测中层水对于应对气候变化带来的挑战以及确保未来世代海洋可持续性至关重要。